Adherence to Bering Strait Vessel Routing Measures in 2019
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The Pacific Gateway to the Arctic: Recent Change in the Bering Strait - Observations, Drivings and Implications
1 The Pacific Gateway to the Arctic: Recent change in the Bering Strait - observations, drivings and implications Rebecca Woodgate, Cecilia Peralta-Ferriz University of Washington, Seattle, USA Recent Change in the Bering Strait New Climatology and Bering Strait products The long-sought “Pacific-ARCTIC” pressure head forcing NASA The Bering Strait, … on a good day Alaska Russia ~ 85 km wide, ~ 50 m deep LOCALLY: - divided into 2 channels by - is an integrator of the the Diomede Islands properties of the Bering Sea - split by the US-Russian - dominates the water border properties of the Chukchi Sea - ice covered ~ Jan - April 8th July 2010 Ocean Color oceancolor.gsfc.nasa.gov (from Bill Crawford) ... influences Important for ~ half of the Russia 80N Marine Life Arctic Ocean Most nutrient-rich watersBarents entering Sea the Arctic (Walsh et al, 1989) Heat to melt ice Fram In spring, trigger western Arctic StraitGreenland melt onset Sea Bering Impacts Global climate stability Year-round subsurface heatStrait Doubling of flow affects Gulf source in ~ half of Arctic Greenland Alaska Stream, overturning circulation (Paquette & Bourke, 1981; Ahlnäs & Garrison,1984; (Wadley & Bigg, 2002; Huang & Schmidt, 1993; Woodgate et al, 2010; 2012) CanadianDeBoer & Nof , 2004; Hu & Meehl, 2005) Archipelago Important for Arctic Stratification Significant part of Arctic In winter, Pacific waters (fresher than Freshwater Budget Atlantic waters) form a cold ~ 1/3rd of Arctic Freshwater (halocline) layer, which insulates the Large (largest?) ice from the warm Atlantic water interannual variability beneath (Wijffels et al, 1992; Aagaard & Carmack, 1989; (Shimada et al, 2001, Steele et al, 2004) Woodgate & Aagaard, 2005) Figure from Woodgate, 2013, Nature Education 4 Overview of Bering Strait measurements MODIS SST 26th Aug 2004 Early 1990s, 2004-2006 == 1+ moorings also in Russian waters. -
Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
A Synthesis of Climate Change and Coastal Science to Support Adaptation in the Communities of the Torres Strait
MTSRF Synthesis Report A Synthesis of Climate Change and Coastal Science to Support Adaptation in the Communities of the Torres Strait Stephanie J. Duce, Kevin E. Parnell, Scott G. Smithers and Karen E. McNamara School of Earth and Environmental Sciences, James Cook University Supported by the Australian Government’s Marine and Tropical Sciences Research Facility Project 1.3.1 Traditional knowledge systems and climate change in the Torres Strait © James Cook University ISBN 978-1-921359-53-8 This report should be cited as: Duce, S.J., Parnell, K.E., Smithers, S.G. and McNamara, K.E. (2010) A Synthesis of Climate Change and Coastal Science to Support Adaptation in the Communities of the Torres Strait. Synthesis Report prepared for the Marine and Tropical Sciences Research Facility (MTSRF). Reef & Rainforest Research Centre Limited, Cairns (64pp.). Published by the Reef and Rainforest Research Centre on behalf of the Australian Government’s Marine and Tropical Sciences Research Facility. The Australian Government’s Marine and Tropical Sciences Research Facility (MTSRF) supports world-class, public good research. The MTSRF is a major initiative of the Australian Government, designed to ensure that Australia’s environmental challenges are addressed in an innovative, collaborative and sustainable way. The MTSRF investment is managed by the Department of the Environment, Water, Heritage and the Arts (DEWHA), and is supplemented by substantial cash and in-kind investments from research providers and interested third parties. The Reef and Rainforest Research Centre Limited (RRRC) is contracted by DEWHA to provide program management and communications services for the MTSRF. This publication is copyright. -
Spanning the Bering Strait
National Park service shared beringian heritage Program U.s. Department of the interior Spanning the Bering Strait 20 years of collaborative research s U b s i s t e N c e h UN t e r i N c h UK o t K a , r U s s i a i N t r o DU c t i o N cean Arctic O N O R T H E L A Chu a e S T kchi Se n R A LASKA a SIBERIA er U C h v u B R i k R S otk S a e i a P v I A en r e m in i n USA r y s M l u l g o a a S K S ew la c ard Peninsu r k t e e r Riv n a n z uko i i Y e t R i v e r ering Sea la B u s n i CANADA n e P la u a ns k ni t Pe a ka N h las c A lf of Alaska m u a G K W E 0 250 500 Pacific Ocean miles S USA The Shared Beringian Heritage Program has been fortunate enough to have had a sustained source of funds to support 3 community based projects and research since its creation in 1991. Presidents George H.W. Bush and Mikhail Gorbachev expanded their cooperation in the field of environmental protection and the study of global change to create the Shared Beringian Heritage Program. -
Inuit People
Inuit People Most of these objects were made in the 19th century by the Inuit, whose name means ‘the people’. The Athabascans called their Inuit neighbours ‘Eskimo’ meaning ‘eaters of raw flesh’. The Inuit way of life was adapted to their harsh territory which stretched 6000 miles across the Arctic from the Bering Sea to Greenland. Carving 80 Chisel handle made from bone with a carved face and animal figures. Possibly from south Alaska, made before 1880. 81 Carrying strap made of hide with a carved stone toggle, made in the 19th century. 82 Smoking pipe made of ivory and decorated with whaling scenes. Made by the western Inuit in the late 19th century. 83 Ivory toggle carved in the form of a seal. Probably made by the western Inuit before 1854. 84 Ivory toggle carved in the form of a bear. Probably made by the western Inuit before 1854. Hunting 85 Snow goggles made of wood. Used in the snow like sun glasses to protect the eyes. Made by the central Inuit before 1831. 86 Bolas made of ivory balls and gut strips, from Cape Lisburn, Bering Strait, made before 1848. Thrown when hunting to entangle a bird or other quarry. 87 Harpoon head, probably for a seal harpoon. Made by the western Inuit in the 19th century. 88 Seal decoy made of wood with claws. It was Used to scratch the ice. The sound attracted seals to breathing holes. Probably made by the western Inuit in the late 19th century. 89 Bone scoop used for clearing seal breathing holes in the ice, made in the 19th century. -
Erosion and Accretion on a Mudflat: the Importance of Very 10.1002/2016JC012316 Shallow-Water Effects
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Erosion and Accretion on a Mudflat: The Importance of Very 10.1002/2016JC012316 Shallow-Water Effects Key Points: Benwei Shi1,2 , James R. Cooper3 , Paula D. Pratolongo4 , Shu Gao5 , T. J. Bouma6 , Very shallow water accounted for Gaocong Li1 , Chunyan Li2 , S.L. Yang5 , and YaPing Wang1,5 only 11% of the duration of the entire tidal cycle, but accounted for 1Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, China, 2Department 35% of bed-level changes 3 Erosion and accretion during very of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA, USA, Department of Geography and 4 shallow water stages cannot be Planning, School of Environmental Sciences, University of Liverpool, Liverpool, UK, CONICET – Instituto Argentino de neglected when modeling Oceanografıa, CC 804, Bahıa Blanca, Argentina, 5State Key Laboratory of Estuarine and Coastal Research, East China morphodynamic processes Normal University, Shanghai, China, 6NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and This study can improve our understanding of morphological Delta Systems, and Utrecht University, Yerseke, The Netherlands changes of intertidal mudflats within an entire tidal cycle Abstract Understanding erosion and accretion dynamics during an entire tidal cycle is important for Correspondence to: assessing their impacts on the habitats of biological communities and the long-term morphological Y. P. Wang, evolution of intertidal mudflats. However, previous studies often omitted erosion and accretion during very [email protected] shallow-water stages (VSWS, water depths < 0.20 m). It is during these VSWS that bottom friction becomes relatively strong and thus erosion and accretion dynamics are likely to differ from those during deeper Citation: flows. -
The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes
1 Surveys in Geophysics Archimer November 2011, Volume 40, Issue 6, Pages 1563-1601 https://doi.org/10.1007/s10712-019-09557-5 https://archimer.ifremer.fr https://archimer.ifremer.fr/doc/00509/62046/ The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes Dodet Guillaume 1, *, Melet Angélique 2, Ardhuin Fabrice 6, Bertin Xavier 3, Idier Déborah 4, Almar Rafael 5 1 UMR 6253 LOPSCNRS-Ifremer-IRD-Univiversity of Brest BrestPlouzané, France 2 Mercator OceanRamonville Saint Agne, France 3 UMR 7266 LIENSs, CNRS - La Rochelle UniversityLa Rochelle, France 4 BRGMOrléans Cédex, France 5 UMR 5566 LEGOSToulouse Cédex 9, France *Corresponding author : Guillaume Dodet, email address : [email protected] Abstract : Surface gravity waves generated by winds are ubiquitous on our oceans and play a primordial role in the dynamics of the ocean–land–atmosphere interfaces. In particular, wind-generated waves cause fluctuations of the sea level at the coast over timescales from a few seconds (individual wave runup) to a few hours (wave-induced setup). These wave-induced processes are of major importance for coastal management as they add up to tides and atmospheric surges during storm events and enhance coastal flooding and erosion. Changes in the atmospheric circulation associated with natural climate cycles or caused by increasing greenhouse gas emissions affect the wave conditions worldwide, which may drive significant changes in the wave-induced coastal hydrodynamics. Since sea-level rise represents a major challenge for sustainable coastal management, particularly in low-lying coastal areas and/or along densely urbanized coastlines, understanding the contribution of wind-generated waves to the long-term budget of coastal sea-level changes is therefore of major importance. -
Shoreline Stabilisation
Section 5 SHORELINE STABILISATION 5.1 Overview of Options Options for handling beach erosion along the western segment of Shelley Beach include: • Do Nothing – which implies letting nature take its course; • Beach Nourishment – place or pump sand on the beach to restore a beach; • Wave Dissipating Seawall – construct a wave dissipating seawall in front of or in lieu of the vertical wall so that wave energy is absorbed and complete protection is provided to the boatsheds and bathing boxes behind the wall for a 50 year planning period; • Groyne – construct a groyne, somewhere to the east of Campbells Road to prevent sand from the western part of Shelley Beach being lost to the eastern part of Shelley Beach; • Offshore Breakwater – construct a breakwater parallel to the shoreline and seaward of the existing jetties to dissipate wave energy before it reaches the beach; and • Combinations of the above. 5.2 Do Nothing There is no reason to believe that the erosion process that has occurred over at least the last 50 years, at the western end of Shelley Beach, will diminish. If the water depth over the nearshore bank has deepened, as it appears visually from aerial photographs, the wave heights and erosive forces may in fact increase. Therefore “Do Nothing” implies that erosion will continue, more structures will be threatened and ultimately damaged, and the timber vertical wall become undermined and fail, exposing the structures behind the wall to wave forces. The cliffs behind the wall will be subjected to wave forces and will be undermined if they are not founded on solid rock. -
Malaysian Journal of Civil Engineering 27 Special Issue (2):325-336 (2015)
Malaysian Journal of Civil Engineering 27 Special Issue (2):325-336 (2015) EVALUATION OF THE WATER AGE IN THE WESTERN PART OF JOHOR STRAIT, MALAYSIA Ziba Kazemi*, Noor Baharim Hashim, Hossein Aslani & Khairul Anuar Mohamad 1 Faculty of Civil Engineering, Universiti Teknologi Malaysia, 81310, Skudai, Johor Bahru, Malaysia *Corresponding Author: [email protected] Abstract: The age of water is useful for understanding the fundamental mechanisms controlling the flux of substances through an estuary. Furthermore, this variable is useful indicators of the susceptibility of estuaries to eutrophication. In this paper, an application of a three-dimensional hydrodynamic model used to evaluate water age distributions for a range of inflow conditions in the Western Part of Strait of Johor, Malaysia. As a first step, the three dimensional hydrodynamic model EFDC was calibrated and then used to evaluate the spatial distribution of water age. Numerical simulations were completed under different inflow conditions. The analysis suggested considerable spatial variation in the water age under both low and high-flow conditions. The average water age in entire system is maximum 14 days under minimum inflow, 194.4 m3/s and minimum 4 days under maximum inflow, 541.3 m3/s. This analysis helped in recognition of areas of the estuary most vulnerable to oxygen depletion and eutrophication. Keywords: Water age, EFDC, hydrodynamic modeling, estuary, Johor Strait. 1.0 Introduction Estuaries are coastal area where freshwater from rivers and streams mixes with saltwater from ocean and are thus characterized by a variety of complicated and complex processes (Michaelis, 1990). One significant and typical estuarine phenomenon is the mixing zone between the saline water and freshwater. -
Successful Breeding of Caspian Terns Hydroprogne Caspia in the Arctic—Part of the New Normal?
Haynes et al.: Caspian Terns breeding in the Arctic 143 SUCCESSFUL BREEDING OF CASPIAN TERNS HYDROPROGNE CASPIA IN THE ARCTIC—PART OF THE NEW NORMAL? TREVOR B. HAYNES, MARGUERITE TIBBLES, KEVIN RODRIGUEZ, BRIAN HAGGERTY PERRAULT & MARTIN D. ROBARDS Wildlife Conservation Society, Arctic Beringia Program, Fairbanks, AK 99775-7000, USA ([email protected]) Received 4 January 2017, accepted 16 May 2017 ABSTRACT HAYNES, T.B., TIBBLES, M., RODRIGUEZ, K., HAGGERTY PERRAULT, B. & ROBARDS, M.D. 2017. Successful breeding of Caspian Terns Hydroprogne caspia in the Arctic—part of the new normal? Marine Ornithology 45: 143–148. Caspian Terns Hydroprogne caspia have expanded their range in the Eastern Pacific, including southern areas of Alaska, over the past several decades. In 2015, we discovered a pair of Caspian Terns on a small gravel island within Krusenstern Lagoon in Cape Krusenstern National Monument and monitored their breeding status until they successfully fledged two chicks. This site is 653 km north of where Caspian Terns had previously been reported to successfully fledge a chick, and represents the first observations of the species breeding above the Arctic Circle or along the Chukchi Sea coastline. The successful fledging of two chicks at Krusenstern Lagoon suggests that this site, and possibly other Arctic sites, can be suitable breeding habitat. Snow cover and sea-ice duration have decreased dramatically in the Chukchi Sea region over the past four decades; as well, seasonal melt-out has become earlier and freeze-up later. As a result of the longer ice-free season, the Arctic may have recently become available as Caspian Tern breeding habitat as it can now accommodate the long breeding season of this species. -
HEAVY MINERAL CONCENTRATION in a MARINE SEDIMENT TRANSPORT CONDUIT, BERING STRAIT, ALASKA by James C
Alaska Division of Geological & Geophysical Surveys PRELIMINARY INTERPRETIVE REPORT 2016-4 HEAVY MINERAL CONCENTRATION IN A MARINE SEDIMENT TRANSPORT CONDUIT, BERING STRAIT, ALASKA by James C. Barker, John J. Kelley, and Sathy Naidu June 2016 Released by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys 3354 College Rd., Fairbanks, Alaska 99709-3707 Phone: (907) 451-5010 Fax (907) 451-5050 [email protected] www.dggs.alaska.gov $3.00 Contents INTRODUCTION .................................................................................................................................................. 1 REGIONAL SETTING ............................................................................................................................................ 2 MATERIALS AND METHODS ................................................................................................................................ 3 RESULTS .............................................................................................................................................................. 5 Heavy Mineral Deposition in the Bering Strait Area .................................................................................... 5 Heavy Mineral Composition ......................................................................................................................... 8 Mineralogy .................................................................................................................................................. -
Waves and Tides the Preceding Sections Have Dealt with the Types Of
CHAPTER XIV Waves and Tides .......................................................................................................... Introduction The preceding sections have dealt with the types of motion in the ocean that bring about transport of water massesin a definite direction during a considerable length of time. They have also dealt with the random motion, the turbulence, which is superimposed upon the general flow. Besidesthese types, one has also to consider the oscillating motion characteristic of waves. In general, this motion manifests itself to the observer more by the riseand fall of the sea surface than by the motion of the individual water particles. Waves have attracted attention since before the beginning of recorded history, and in recent years they have been the subject of extensive theoretical studies. Surveys of our knowledge as to the character of ocean waves have been presented by Cornish (1912, 1934), Krtimmel (1911), Patton and Mariner (1932) and by Defant (1929). Lamb (1932) has discussed the hydrodynamic theories of waves, and Thorade (1931) has given a comprehensive review of the theoretical studies of ocean waves and has compiled a long list of literature covering the period from 1687 to 1930. Our understanding of the waves of the ocean, how they are formed and how they travel, is as yet by no means complete. The reason is, in the first place, that actual observations at sea are so difficult that the characteristicsof the waves cannot easily be determined. In the second place, the theories that serve to bring the observed sequence of events in nature into intimate connection with experience gained by other methods of study are still incomplete, particularly because most theories are based on classicalhydrodynamics, which deal with wave motion in an idealized fluid.